Geology Chapter 3 Flashcards
magnitude
the amount of energy released
intensity
the effects of ground motion on people and structures
earthquake cycle
a drop in elastic strain after an earthquake and a re accumulation of strain before the next event
p waves
compressional or primary waves
-can travel through solid,liquid, and gas
s waves
shear or secondary waves can travel only through solid materials
surface waves
form and move along Earth’s surface
tectonic creep
gradual movement along the fault
fault
is a fracture or fracture system where rocks have been displaced;the Earth’s crust on one side of the fracture or fracture system has moved relative to the other side
liquefaction
intense shaking can cause a near-surface layer of water saturated sand to change rapidly
material amplification
strongly influences the amount of ground motion experienced
modified mercalli scale
- 12 categories on this scale are assigned roman numerals
- each category contains a description of how people perceived the shaking
moment magnitude
is determined from an estimate of the area that ruptured along a fault plane during the earthquake
the amount of movement or slippage and the rigidity of the rocks near the focus of the quake
epicenter
is the place on the surface of Earth above where the ruptured rocks broke to produce the earthquake
focus or hypocenter
directly below epicenter